Abstract
On materials of laboratory and expeditionary researches on the cooling pond of the Zaporizhya nuclear power plant and adjoining area of the Kachovka reservoir are found out features of temperature and oxygen regime of the cooling ponds and condition and factors, that them determine. Carried out researches testify to significant thermal loading on ecosystem of the cooling pond which determines a course of hydrobiological and physico-chemical processes. Differences of the hydrochemical regime of cooling ponds from similar reservoirs in natural conditions are caused, first of all, by features of their thermal regime. Because of constant artificial heating, character of hydrobiological, physico-chemical and hydrodynamical processes in cooling ponds are formed peculiar conditions of formation of the dissolved oxygen regime.
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